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New class of comets may be source of Earth's waterUNIVERSITY OF HAWAII NEWS RELEASEPosted: March 23, 2006

Three icy comets orbiting among the rocky asteroids in the main asteroid belt between Mars and Jupiter may hold clues to the origin of Earth's oceans.

Three known main-belt comets are seen in the center of each panel) Other objects shown are stars and galaxies smeared by the motion of the telescope while tracking each comet. Images taken with the UH 2.2-meter telescope by H. Hsieh and D. Jewitt (Univ. Hawaii).

The newly discovered group of comets, dubbed "main-belt comets" by
University of Hawaii graduate student Henry Hsieh and Professor David
Jewitt, has asteroid-like orbits and, unlike other comets, appears to have
formed in the warm inner solar system inside the orbit of Jupiter rather
than in the cold outer solar system beyond Neptune.

The existence of these main-belt comets suggests that asteroids and comets
are much more closely related than previously thought and supports the
idea that icy objects from the main asteroid belt could be a major source
of Earth's present-day water. This work is scheduled to appear in the
March 23 edition of Science Express and in an April print edition of
Science.

The crucial observations were made on November 26, 2005, using the 8-meter
Gemini North Telescope on Mauna Kea. Hsieh and Jewitt found that an object
designated as Asteroid 118401 was ejecting dust like a comet. Together
with a mysterious comet (designated 133P/Elst-Pizarro) known for almost a
decade but still poorly understood, and another comet (designated P/2005
U1) discovered by the Spacewatch project in Arizona just a month earlier,
"Asteroid" 118401 forms an entirely new class of comets.

"The main-belt comets are unique in that they have flat, circular,
asteroid-like orbits, and not the elongated, often tilted orbits
characteristic of all other comets," said Hsieh. "At the same time, their
cometary appearance makes them unlike all other previously observed
asteroids. They do not fit neatly in either category."

In both 1996 and 2002, the "original" main-belt comet, 133P/Elst-Pizarro
(named after its two discoverers), was seen to exhibit a long dust tail
typical of icy comets, despite having the flat, circular orbit typical of
presumably dry, rocky asteroids. As the only main-belt object ever
observed to take on a cometary appearance, however, 133P/Elst-Pizarro's
true nature remained controversial. Until now.

"The discovery of the other main-belt comets shows that 133P/Elst-Pizarro
is not alone in the asteroid belt," Jewitt said. "Therefore, it is
probably an ordinary (although icy) asteroid, and not a comet from the
outer solar system that has somehow had its comet-like orbit transformed
into an asteroid-like one. This means that other asteroids could have ice
as well."

The Earth is believed to have formed hot and dry, meaning that its current
water content must have been delivered after the planet cooled. Possible
candidates for supplying this water are colliding comets and asteroids.
Because of their large ice content, comets were leading candidates for
many years, but recent analysis of comet water has shown that comet water
is significantly different from typical ocean water on Earth.

Asteroidal ice may give a better match to Earth's water, but until now,
any ice that the asteroids may have once contained was thought to either
be long gone or so deeply buried inside large asteroids as to be
inaccessible for further analysis. The discovery of main-belt comets means
that this ice is not gone and is still accessible (right on the surfaces
of at least some objects in the main belt, and at times, even venting into
space). Spacecraft missions to the main-belt comets could provide new,
more detailed information on their ice content and in turn give us new
insight into the origin of the water, and ultimately life, on Earth.

As conventionally defined, comets and asteroids are very different. Both
are objects a few to a few hundred miles across that orbit throughout our
solar system. Comets, however, are thought to originate in the cold outer
solar system and consequently contain much more ice than the asteroids,
most of which are thought to have formed much closer to the Sun in the
asteroid belt between Mars and Jupiter.

Comets also have large, elongated orbits and thus experience wide
temperature variations. When a comet approaches the Sun, its ice heats up
and sublimates (changes directly from ice to gas), venting gas and dust
into space, giving rise to a tail and a distinctive fuzzy appearance. Far
from the Sun, sublimation stops, and any remaining ice stays frozen until
the comet's next pass close to the Sun. In contrast, objects in the
asteroid belt have essentially circular orbits and are expected to be
mostly baked dry of ice by their confinement to the inner solar system.
Essentially, they should be just rocks. With the discovery of the
main-belt comets, we now know this is not the case, and that, in general,
the conventional definitions of comets and asteroids are in need of
refinement.

This work is supported by a grant from the NASA Planetary Astronomy
Program of the Science Mission Directorate.